Chemical and boron isotopic compositions of tourmaline at the Dachang Sn-polymetallic ore district in South China: Constraints on the origin and evolution of hydrothermal fluids.

MLA

Zhao, Kui-Dong, et al. “Chemical and Boron Isotopic Compositions of Tourmaline at the Dachang Sn-Polymetallic Ore District in South China: Constraints on the Origin and Evolution of Hydrothermal Fluids.” Mineralium Deposita, vol. 56, no. 8, Nov. 2021, pp. 1589–608. EBSCOhost, https://doi.org/10.1007/s00126-021-01045-4.

APA

Zhao, K.-D., Zhang, L.-H., Palmer, M. R., Jiang, S.-Y., Xu, C., Zhao, H.-D., & Chen, W. (2021). Chemical and boron isotopic compositions of tourmaline at the Dachang Sn-polymetallic ore district in South China: Constraints on the origin and evolution of hydrothermal fluids. Mineralium Deposita, 56(8), 1589–1608. https://doi.org/10.1007/s00126-021-01045-4

Chicago

Zhao, Kui-Dong, Ling-Huo Zhang, Martin R. Palmer, Shao-Yong Jiang, Cong Xu, He-Dong Zhao, and Wei Chen. 2021. “Chemical and Boron Isotopic Compositions of Tourmaline at the Dachang Sn-Polymetallic Ore District in South China: Constraints on the Origin and Evolution of Hydrothermal Fluids.” Mineralium Deposita 56 (8): 1589–1608. doi:10.1007/s00126-021-01045-4.